noranda exploration company, limited · 2017-01-17 · noranda exploration company, limited (no...

53K15NEaei6 2.18185 SLATE LAKE 010

NORANDA EXPLORATION COMPANY, LIMITED (no personal liability)

REPORT OF WORK - 1986

PANAMA LAKE PROPERTY

N.T.S. 52K/15

NORTHWESTERN ONTARIO DIVISION

l; l.C-H

, A M TIC ^T'ONffp'NR l-VM'S ot-"'-' 1 *l * 11 s * j '

PROJECT 1332 THUNDER BAY, ONTARIO JANUARY 23, 1987

PAUL DEGAGNEGEOLOGIST

RED LAKE DISTRICT

r/i ' tf

52K15NE0816 2.10185 SLATE LAKE 010C

Table of Contents

I.0 INTRODUCTION

2.0 LOCATION, ACCESS AND TOPOGRAPHY

3.0 DESCRIPTION OF PROPERTY

4.0 PROPERTY HISTORY

5.0 REGIONAL GEOLOGY

6.0 PROPERTY GEOLOGY

6.1 Description of Units

6.2 Structure and Stratigraphy

7.0 HUMUS SAMPLING PROGRAM

8,0 GEOPHYSICS

9.0 MINERALIZATION

10.0 CONCLUSIONS

II.0 RECOMMENDATIONS

12.0 REFERENCES

13.0 STATEMENT OF QUALIFICATIONS

Page

l

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1

2

2

2

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7

8

9

10

List of Attachments

n FIGURE l

FIGURE 2

MAP l

MAP 2

MAP 3

LOCATION MAP

CLAIM MAP

PROPERTY GEOLOGY

HUMUS SAMPLE RESULTS

MINERALIZED ZONE

Scale

1:250,000

l" n l mi

1:5000

1:5000

1:500

1.0 INTRODUCTION

The Panama Lake property was staked in July 1986, after reconnaissance sampling of an old trench returned anomalous gold values.

During the summer and fall of 1986, a grid was cut on the property and detailed mapping, humus sampling, Magnetometer and VLF (EM-16R) surveys were conducted in order to determine the nature and extent of the gold mineralization.

2.0 LOCATION AND ACCESS

The property is located approximately 56 kms northeast of the Town of Ear Falls which is situated on Highway 105, 70 kms south of the Town of Red Lake (Figure 1).

At present, access to the property is by ski or float- equipped aircraft. Great Lakes Forest Products Ltd is currently active in the area and the all-weather Wenesaga Lake road passes within 5 kms of the property, the Ben Lake road, an offshoot of the Wenesaga Lake road, currently reaches a point approximately 4.5 kms west of the property and is being extended towards our claims.

Outcrop is extensive along the northern claim boundary and in the western half of the property. Forest cover in these areas consists of black spruce and poplar with thick alder growth along the numerous creeks which crosscut the property. The eastern half of the claim block is underlain by muskeg swamp with thick growths of black spruce and alder. The four claims located south of Panama Lake are situated along a large east-west trending ridge of thick till and sparse outcrop. Forest cover in this area is poplar and spruce.

3.0 DESCRIPTION OF THE PROPERTY

The Panama Lake property consists of 28 unpatented mining claims in the Red Lake Mining District (Figure 2). The claims are numbered as follows:

CLAIM NUMBERS

KRL 926983-986, inclusive KRL 927017-018, inclusive KRL 939098-119, inclusive

The claims are outlined on Claim Map G.1884 - Slate Lake Area.

A

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UCHI JL.A'KE^Gand - ~

EARN'GEY TWP.

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is d A x r*' - ~r r ^^- ,

.' 7 i -- '- ; .^ ^t *. . . - --* i ~ ' ' . '\ . *, ~ .. . ' " * \ - ' "v'V

1 ^

4.0 PROPERTY HISTORY

The Panama Lake area has been mapped several times by Ontario government geologists (Bateman, 1939; Bowen, 1980, Preliminary Map P.1200), A joint ODM-GSC aeromagnetic survey of the area was published in 1960.

The only work recorded of the property was performed in the late 1940's. In 1945, J, Pemican and J. Hager staked 8 claims on the north shore of Panama Lake. The claims were transferred to Peraican Mines Limited which performed surface work and reportedly 1500' of diamond drilling in 1946. the drilling returned negative results. A diamond drill hole collar (Azimuth 325 0 , Dip -45 0 ) was located on Line 6E/0+75S but it seems unlikely that this hole could have reached the exposed mineralized structure. Grab samples from an old trench located on Line 7E/0+25N reportedly returned gold values ranging from trace to 0.26 opt.

Numerous companies (including Dome, St.Joseph, Halren Mines and Keevil Mining Group) were active in the immediate vicinity of the Panama Lake property from the late 1960's to the early 1980's. Ground magnetic and electromagnetic surveys, followed by diamond drilling, were performed on the properties. All results were negative.

5.0 REGIONAL GEOLOGY

The Panama Lake property is situated in the southern part of the Archean Birch Lake-Uchi Lake Greenstone Belt, an east-trending assemblage of metavolcanic and metasedimentary rocks.

In the immediate Panama Lake area, the belt trends northeasterly and consists mainly of clastic metasediments to the southeast of Panama Lake and felsic to mafic metavolcanic rocks and large gabbroic sills northwest of the property.

A series of northeast-trending synclinal fold axes pass 2 kms west of the property and the Uchi Lake Fault lies 4 kms to the north. The fault shows little stratigraphic offset but brecciation, silicification, carbonatization and a well developed schistosity of the rocks are observed in the immediate area. These features are also apparent along both shores of Slate Lake, suggesting that a major fault or shear zone may underly the lake.

6.0 PROPERTY GEOLOGY (Map 1)

6.l Description of Units

Unit l - Mafic VolcanicsThis unit crops out as a thin, northeast trending sequence in

the northwest part of the property. The rock is typically dark green, aphanitic and massive to pillowed. Pillows are small, bun shaped and tops could not be determined.

Unit 2 - Intermediate TuffThis unit underlies approximately 6QZ o f the property. It is

generally a thinly bedded, fine-grained, waterlain tuff which can be locally quite silty or interbedded with thin chert laminae. The intermediate tuff is commonly light grey to pale green, strongly foliated and consists largely of quartz and sericite. Trace pyrite and calcite alteration is found throughout the unit.

Unit 3 - Banded Argillite-GreywackeA thin wedge of argillite-greywacke crops out in the

northeastern corner of the property. The unit is fine grained, thinly laminated and grey to brown in colour. These sediments form the western extent of a thick sequence of metasediments that extends to the north and east of Jubilee Lake.

Unit 4 - Magnetite Iron FormationA single band of magnetite iron formation occurring within

the intermediate tuff was located between Lines 5E andSE/0+25 to 0+50N. The unit trends approximately 060 0 and is up to 5m thick where exposed. Magnetic data suggests this unit extends as far west as L3+25E and off the eastern edge of the property at L24E/200-300N. A break in the magnetic trend at 9*50E,100N suggests the presence of a northwest trending fault passing through this location. The rock is black, fine grained and contains up to 3% disseminated pyrite. It is poorly bedded and has a high argillaceous component.

Unit 5 - Mafic TuffOn the northeast shore of Panama Lake (L14-16E) several

outcrops of mafic tuff were noted. The rocks are similar in nature to the intermediate tuffs which underlie most of the property but are green in colour due to their higher mafic content.

Unit 6 - GabbroThe northeastern part of the property is underlain by a large

gabbroic sill which may in part be coarse grained flows. It is medium to coarse grained, equigranular and composed of plagioclase and amphibole (hornblende). Numerous thin, fine-grained, aphanitic, mafic dykes occur throughout the property and are probably fine-grained equivalents of the gabbro.

6,2 Structure and Stratigraphy (Map 1)

Regional mapping by government geologists suggests that stratigraphic tops in the area are to the south.

The Panama Lake property is underlain by a north to south succession of massive to pillowed mafic flows, intermediate waterlain tuffs, and argilliceous metasediments. These units have been intruded by a large gabbroic sill to the north. Thinly laminated fine-grained

sections with a high sedimentary component within the intermediate tuffaceous sequence suggest a distal waterlain origin for these rocks. The sedimentary wedge at the eastern edge of the property may be time- equivalent with the tuffs.

All units appear to strike northeast and dip steeply south. Foliation exhibited within the tuffaceous metavolcanics parallel these trends.

The only major structural feature of the property is a shear zone exposed between lines 6E and 8E between 0+25 and 0+50N. This zone trends 060 0 , plunges 50 0 to 70 0 to the west, exhibits intense silicification of the host tuff, and carries anomalous gold values.

7.0 HUMUS SAMPLING PROGRAM (Map 2)

A humus sampling program was conducted on the Panama Lake property in an attempt to delineate the gold-bearing shear zone beneath overburden. A total of 315 humus samples were collected and analyzed for gold. The results are shown on Map 2.

Four samples returned very anomalous gold values. One of these values (198 ppb) is located directly over the exposed mineralized zone. The other three (41, 33 and 16 ppb) are located to the west and somewhat along strike of the zone. Above background values of 5 to 10 ppb parallel the trend of the structure both to the eastern and western edges of the property.

8.0 GEOPHYSICS

Magnetometer and VLF (EM-16R) surveys were conducted on the Panama Lake property (a detailed report on these surveys is forthcoming).

The magnetometer survey outlined the gabbroic sill in the northwest and the iron formation in the central part of the property. The iron formation appears to extend from L3+23E on the baseline to the eastern edge of the property (L24E/100-200N) and has apparently been faulted along a northwest-trending break at L9+50/1+OON.

The VLF (EM-16R) survey outlined a zone of high resistance between L34-50E on the baseline and L9+50E which corresponds to the mineralized silicified shear zone. Truncation of the resistive zone to the east may be due to the northwest-trending fault mentioned previously. The loss of the resistive zone to the west may be due to an increase in overburden cover.

9.0 MINERALIZATION (Map 3)

Gold mineralization on the property appears to be related to a northeast-trending shear zone exposed between lines 6E and 8E from 0+25 to 0+50N. This zone trends 060 0 , dips vertically to steeply south and appears to plunge 50-70 0 to the west. It has an exposed width of up to lOra. The zone is characterized by intense silicification, sericitization, and moderate tourmaline enrichment. Pyrite is disseminated throughout the zone in amounts ranging from trace to 0.57,.

A total of 27 grab, 31 hand chip and 116 channel samples were collected from 16 hand-stripped sites across the zone. The location of these sites and the average values from each of the channel sample locations are shown on Map 3. Table l lists the values for the grab and chip samples.

Gold values ranged from trace to 11.25 g/t and are quitevariable throughout the zone. Several of the high values that wereobtained from the early grab and chip samples could not be repeatedwith the channel samples and are probably due to a nugget effect.

Samples of the intermediate tuff taken immediately adjacent to the silicified zone carried only trace gold. Several samples of iron formation exposed near the structure were sampled with poor results in spite of the moderate sulphidization to pyrite.

Within the zone itself, gold mineralization appears to be randomly distributed and does not seem to be related to a specific horizon or zones of pyrite or tourmaline mineralization.

TABLE l

(GB - Grab, CP - Chip)

Sample

373713737337372313373737637374373753133431335313363737837379373803737737381

Strip Site f

l l l122222233334

Sample Type

GB GB CP CP GB CP CP CP CP CP GB GB GB CP GB

Sample Length (m)

n/a

.5

.5

1.0 1.0 1.0 1.0 0.6

0.75

Au 8/t

5.6 tr. 4.4 5.6

1.3 tr. 1.9 tr. tr. tr. tr. tr. tr. tr.

TABLE l (cont'd)

Sample

37382373863738738383373843738537388373893739037307373083730937310373113731237313373143739437395373913739237393313463134738348383493835037397373963740037398373993740137402374033136337405374043740737406373043730537306374083730337409

Strip Site j?

45555566677777777777777777788999

1010101011111212131313131414

Sample Type

GBGBGBCPCPCPCPCPCPGBGBGBGBGBGBGBGBGBGBCPCPCPCPCPCPCPCPGBCPGBCPCPCPCPCPGBGBGBGBCPGBGBGBCPGBCP

Sample Length (m)

1.5 1.8 1.5 1.5 1.5 1.2

1.20.50.90.30.151.100.700.35

2.0

2.0 1.0 0.9 0.9 1.5

1.0

1.0

0.6

Au 8/t

tr. tr. tr. tr. tr. tr. 4.0 2.3 2.8 6.25

1.9 11.3 8.8 5.6 tr . 0.3 tr. tr. 3.1 2.5 3.1 tr. 1.3 3.8 0.6 3.8 tr. 2.5 tr. 3.1 6.3 3.1 0.3 tr. 1.9 1.9

14.4 tr. 3.8 0.3 1.9 0.3 3.8 tr. tr.

10.0 CONCLUSIONS

Gold mineralization has been found along a shear zone which

cuts through an intermediate tuffaceous sequence. The zone trends

060 0 , dips vertically to steeply south and appears to plunge 50-70 0 to

the west. It has an exposed strike length of 250m, an exposed width of

10m and lies between L6+OOE/0+25N and L8+50E/0+50N. The rocks in this

shear zone have undergone intense silicification and sericitization,

and moderate tourmaline enrichment. Disseminated pyrite occurs

throughout the silicified rocks in amounts up to G.5%.

Gold values range from trace to 14.4 g/t with the best

channel sample result being 10.3 g/t over l.lm. The average grade over

the length of the entire zone, based on 131 channel samples, is

approximately 3 g/t. Similar structures at the nearby Uchi and

Jackson-Manion Mines contained a series of high grade offshoots which

produced 141,500 ounces Au.

The VLF survey suggests the zone extends as far west as

L3+50E on the baseline, and as far east as 9+50E/0+75N where it may be

faulted off.

The extensive iron formation indicated in two exposures and

by the magnetometer survey, may be crosscut at a low angle by the

mineralized structure and therefore represents a prime target for

replacement gold mineralization. Such an occurrence might be expected

to have a higher grade than the structure itself*

11.0 RECOMMENDATIONS

1) The shear zone should be tested at a depth of 150-200m by several

diamond drill holes along its length. One hole should target the

western part of the structure where it intersects the iron formation.

2) Both the western and eastern extensions of this zone should be

prospected in more detail, particularly in the vicinity of the humus

anomalies.

3) On a regional scale, the shear zone may be part of a larger fault

or shear zone. Evidence for this is the alignment of the zone with the

north shores of Upper Slate Lake, Panama Lake, Anape Lake and Ben

Lake. These areas should be prospected for similar zones of gold

mineralization.

Respectfully submitted

NORANDA EXPLORATION COMPANY, LIMITED (no personal liability)

Paul Degagnef , Thunder Bay, Ontario Geologist-Red Lake District i' January 23, 1987 Northwestern Ontario Divisionli

I, PAUL DEGAGNE, hereby certify

1. I ara a practicing geologist with Noranda Exploration Company, Limited in Thunder Bay, Ontario, and reside at 84 Elizabeth Street, Thunder Bay, Ontario.

2. I am a graduate of Laurentian University, Sudbury, Ontario, 1982, with a degree of Bachelor of Science.

3. I am a Canadian citizen.

I have practiced my profession for approximately 5 graduation.

years since

I do not have, nor do I expect to receive, directly or indirectly, any interest in the properties of Noranda Exploration Company, Limited.

Dated at Thunder Bay, Ontario, this 23th day of January, 1987

Paul DegagneGeologistNorthwestern Ontario Division

10

2::ploration Ltd.

Pi 2 2 CUSTOM FIRE ASSAYINo LTD.

PAULOKANSKI.Assayer Box 253, Cochenour, Ontario POV l LO

" ASSAY CERTIFICATE

Phone: Bus. (807)'662-8171 Res. (807) 662-3361

/ g J. Date: July 17-36

l

2

3

4

5

6

7

8

9

10

11

12

Sample No.

37470 '

71

72

73

74

75

76

77

78

79

00

yl

Description

Troj. -."--1313-7x5- 15

,

-

oz/ton Au

Trace

it

ii

H

ti

M

ii

n

ii

ii

n

it

oz/ton Ag

17

18

19

20

21

22

23

24

25

or

0-7

83

89

90•r" - 9r

92

93

94

95

,

M

n

n

it

H

H

n

n

M

.01

REPORT: oie-4?89 ( COMPLETE ) REFERENCE IKFO:

CLIENT: NORANDA EXPLORATION CO. LTD. PROJECT: 1322-EZ-15

SUBMITTED BY: IftN PERRY HATE PRINTED: 3-DEC-86

ORDER ELEMENT

l Au Gold

NUMBER OF LOWERANALYSES DETECTION LIMIT EXTRACTION

315 l PPB

METHOD

Neutron Activation

SAMPLE TYPES

ORGANIC OS HUMUS

NUMBER

31?

SIZE FRACTIONS

-10

NUMBER

317

SAMPLE PREPARATIONS

BRIQUET T ING SHRINK MAPPING SIEVE -10

NUMBER

311 311 311

REMARKS: < MEANS LESS THAN.

REPORT COPIES TO: I. PERRY INVOICE TO: I. PERRY

(fi

\ Ud.i**;; •tf:.

S^-" ^gmW^JSfltBQNDARrCLEGG Geochemical

Lab Report

"REPORT: 01 6-4789 PROJECT: 1322-Ez-is PAGE i jSAMPLE ELEMENT NUMBER UNITS

Au PPB

SAMPLE EEMENI NUMBER UNITS

Au iPPB i

LO+QOE-0+00 LO+OOE-0+25N LO+OOE-0+50N LOtOOE-Oi75N LO+OOE-1400N

2 4 3 71

12+OOE-0+OON L2+OOE-0+25S L2+OOE-0+50S l2*OOE-Ot75S L2+OOE-1+OOS

4r^W- ••••-- ^ |

. 4';. : ;V" ' i

aLO+OOE-H25N LO+OOE-1+50N

: :: LOtOOE-lt75N . ; LOtOOE-2tOON

- ; LO+OOE-2+25N

4 2

•^'••S.'a

L2+OOE-H25S L2+OOE-1+50S "" L2+OOE-1+75S 13+OOE-1+50N fcC

,. . ' ' : , . L3+OOE-1+25M '-;:|S?;!- :

. 2 ;. .-..; ; .. , ; - . -

a -. .. :;-'-;. -.': ' . , .' - , ', .^'.•; ' : --.

10+OOE-2+50N LOtOOE-2*75N

" — LO+OOE-3+OON LO+OOE-3+25N LO+OOE-3+50N

3

2

L3+OOE-HOON L3+OOE-0+75N : 13+OOE-OtSON L3+OOE-0+25H 13+OOE-O+OON

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3 2 3 2 2

L3+OOE-0+25S L3+OOE-0+50S

i L3t00E-(H75S L3*OOE-1*OOS 13+OOE-1+25S

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•: L2+OOE-4+50N L2+OOE-4+25N L2+OOE-4+OON

46

5 2

L3+OOE-1+50S 13+OOE-1+75S L3+OOE-2+OOS -i ; L4*OOE-1*50N :' A L4+OOE-U25N }: i

:a... ,: :;;^.-, , .;^.. - ; ^/: 2 i-: îjjfy^^M'- ;i\..

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L2*OOE-3t75N L2+OOE-3+50N

, L2tOOE-3*25N •- ' L2+OOE-3+OON , ; - :: : L2tOOE-2*75N i.

4 2 3

L4*OOE-UOON L4*OOE-0*75H " L4*OOE-0*50N i14+OOE-0+25N i- i

- . ;. * j , ... ; :'; v L4+OOE-0+OON /H^'V

rÎ .^^ftC.^. , • •-'.•': *Q*'-'-'f'VyZ^:':-f-'.-- "•'•'.- :'."

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. . ; L2+OOE-2+50N ; 'i-- ; L2+OOE-2+25N

:: L2+OOE-2+OON - v - ; - L2+OOE-1+75N ;

V :' K^'Iv L2+OOE-U50N ;^

.;- ': fl ...- '

t-'-'l ' ' 0 ' v- ' ' . iijrf t J l*'- '

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L2+OOE-1+25N " . L2+OOE-1+OON ;:

L2+OOE-0+75N L2+OOE-0425N A L2+OOE-0+25N B

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4

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Geochemical Lab Report

'

REPOtT: 016-4789 PROJECT: i322-EZ-is PAGE 2SAMPLE ELEMENT NUMBER UNITS

Au PPB

SAMPLE ELEMENT NUMBER UNITS

Au PPB

L5400E-1400N L5400E-0475N 15400E-0+50N

ffi/. 154-OOE-0+25N L5+00E-0400N

2 2

16

L8400E-HOON L8400E-0475N L8400E-0450N L8400E-0425N

^ L8+OOE-0400

3 2 1

ffi L5400E-0+25S ffi'-; . L5400E-0475S

- -# ffi -ffi L5400E-HOOSffi-. ffi: ffi^-' L5400E-1425S

4 ; -?f"y . L5400E-1450S

3 1 3

3

L8400E-0425S L8400E-0450S L8+OOE-0475S ^L8400E-HOOS ffi^I L9400E-2425N ffilS

1a aXI

.•:"..;2.; ffi'. .-:- ' . .,.

: L6400E-1450N L6+OOE-U25N

— " : : L6400E-HOON 16400E-0475N L&400E-0450N

3.a

2a

2

L9400E-240WI ffi L9400E-14758 L9400E-1450N L9400E~1425N L9400E-UOON

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L6400E-0425N L6400E-0400N L6400E-0425S L6400E-0450S L&400E-0475S

a4

3 2

L9400E-0+75N L9400E-0450N L9400E-0425H L9400E-0400 L9+00E-0425S

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- ";.;';.v.;J' . . '-. .

. L6400E-U00S - L7400E-2425N

: ^ v L7400E-2400N ffi. ffi L7+OOE-1+75N , "tffi-ffi 17400E-1+50N

3a a a a

L9400E-0450S L9400E-0475S L9400E-1400S ffi X L10400E-2400N 'ffi L10400E-1475N ffi

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, iffiA L7+OOE-U25N ' .I7400E-1+00N

' v ; L7+OOE-0+75N .. L7+00E-0+50N

. r-, : ; I7+OOE-0+25N

4i5 6

198.-:

L10400E-1450N .ffijffi; 110400E-1425N ;' :i 1 L10400E-1400N ,ffitKj;

7 -,ffiv-; ;'.v,:,:- i";V . ffi :

. ffi-. , L7+OOE-0+00 BL : \* : : 17+OOE-0+25S ffi

:- L7400E-0+50S- •.' .-. L7+OOE-0+75S

L7+00E-HOOS

4a3a

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: . ' ; : . - .-'. ffi ^^\ ffi'.; 110400E-0475S :-W^r"|-;

: L8+OOE-2+25N ' : L8+OOE-2+OON ,\ ffi ffi L8+00E-1475N

•'-y-. '.V L8400E-1450N - V '. L8+OOE-1425N

2 2

2

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"one 3 M\J^ '0 i^^ytS T kx: OSJjS^ "

it-Hi BONDAR- CLEGGnu ^J^yjigiffll jy JH jjfc^mjft^^ajymiati

Geochemical Lab Report

life.

'

REPORT: oie-4789 l PROJECT: 1322-EZ-15 PAGE 3


Au PPB


Au PPB

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2 V

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a

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—— ' L12tOOE-l*25N L12+OOE-1+OON L12^00E-Ot75N

2

a i

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3 3 3a

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REPORT: 016-4799SAMPLE ELEMENT NUHBER UNITS

. L20*OOE-3tOON L20*OOE-2t?5N L20+OOE-2+50N L20+OOE-2+25N L20+OOE-2+OON

.,, :L20tOOE-l*75N : - ' L20+OOE-1+50N

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L20+OOE-0+50N L20+OOE-0+25N

. 120+OOE-OtOO L20+OOE-0+25S L20tOOE-0*50S

L20+OOE-0+75S L20tOOE-HOOS

. L20+OOE-1+25S L20+OOE-1+50S L20+OOE-1+75S

L20+OOE-2+OOS L20tOOE-2t25S

: L20+OOE-2+50S - , L20+OOE-2+75S

L20+OOE-3+OOS

. L20+OOE-3+25S ' ' - 120+OOE-3+50S Y . . 120+OOE-3+75S ;; , L20+OOE-4+OOS

..; ," ; ; L22+OOE-2+75R ; ; ;

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a a

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PROJECT: i322-EZ-is PAGE 4SAMPLE ELEMENT Au NUHBER UNITS PPB

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L22+OOE-0+50S 4 : L22*OOE-0*75S 6

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HOntario

Report of Work

iG'.'op'v.s c.r. Geoioi|.Ciii.G'.'OChvl" C.i. .ilUl Exp'MllllUr ho

S2K15NE0016 2.10)65 SLATE LAKE900

Note

Mininfl Actvpe of 5'Jfvo ' s

Benificiation (Humus, Rock samples)Cl.l.m HOUJO' ;S'

Noranda Exploration Company, Limited

P.O. Box 2656, Thunder Bay, Ontario P7B 5G2Survey Company

Noranda Exploration Company, Limited

Slate Lake AreaPfO'i::- 0 '' *or's L pp L

A 34387No

Name and Address of Author (of Geo Tecimcal reportl

Paul DeGagne, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2

fOnic o* S ufwov if'om Ut l o!

;D.iy i Mo. l Yr. j Day i Mo Y r.

Tota: Miles o* l.ne Cut13.25

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

G , Days per Claim

- Electromagnetic i

- Magnetometer

- RacJiomeiric i

- Other

Geological

Geochemical

Man Days

Complete reverse si and enter totarftJ^J

** , *

toeoonys.cal

'Electromagnetic i

r*

jV^- Other

Geological

Geochemical

Airborne Credits

Note: Special provisions ! Electromagnetic credits do not apply

Days per Claim

to Airborne Surveys. Magnetometer

Radiometric

Expenditures {excludes power stripping)Type of Work Performed

Humus - Rock samplesPerformed on Claim(s)

KRL. 939099-939101, 939104-939111,

939115, 926983-926986, 927017.Calculation of Expenditure Days Credits

Total ExpendituresTotai

Days Credits

S 2822 ~- 1 5 =

InstructionsTotal Days Credits may bo apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

^Prefix

.ML.^

lining ClaimNumber

^927018.. -. 939112

...939113 .... .

^93911.4......

939115

939116

..959.117

939.1.18... ..

-339119

.--.— - —— — - -

Exp.-id.Days Cr.

JQ.A 20.8

2.0,^ .20.. 8...

20.8

20.8

20.8

'-^r

— . —

^''

V

^

Mining Claim

Prel ix Numberj

.. ; . - . .. .

j

iiii

i

3^i *

^:::::::--..L' t

Toiol number of mining claims covered by this l report of work.

Expend.Days Cr.

- --— -

- ——— ——

———— ——

)

Dat*

June 25,1987Recp*Ood Holdep or ^ Signature l

Certification Verifying Ffeport of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed jame during and/or after its completion and the annexed report is true.

jName and Postal Address of Person Certifying

lan Perry, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2 ^

' 1 2.7 O 1 ~]Date CertifiedJune 25,1987

Ministry ofNorthern Development

Minos

Technical Assessment Work Credits

Date

September 21,1987

File

2.10185Mining Recorder'1 Report of Work No.

64-87

Recorded HolderNoranda Exploration Company Limited

Slate Lake Area

Type of survey and number of Assessment days credit per claim

Geophysical

electromagnetic riays

Section 77 (19) See "Mining Claims Assessed" column

Geological -~ 1--' riays

--20 -Geochemical riays

Man days L~3 Airborne | ]

Special provision [3 Ground [x!

l 1 Credits have been reduced because of partial coverage of claims.

| | Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

KRL 939118 -119 inclusive

Special credits under section 77 (16) for the following mining claims

5 Days Geological 10 Days Geological 15 Days GeologicalKRL 927018 KRL 939117 KRL 939115 -116

939114

Mo credits have been allowed for the following mining claims

| | not sufficiently covered by the survey | | insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.

828 (85/12)

Ministry ofNorthern Development •"l Mines


DateSeptember 21,1987

File

2.10185Mlnlno Rocorder'i Report of Wor k *o. 6 5-87

Recorded Holder

Noranda Exploration Company, LimitedTownship or Area

Slate Lake

Type of survey and number of Assessment days credit per claim

Geophysical 20

20


40fipnlngiral riays

Man days | | Airborne (~l

Special provision [^ Ground (XJ

| l Credits have been reduced because of partial coverage of claims.



KRL 939102 - 103

Special credits under section 77 (16) for the following mining claims15 Days Electromagnetic S Magnetometer 5 Days Electromagnetic S Magnetometer

S 40 Days Geology S 10 Days GeologyKRL 939098 KRL 939112

93910110 Days Electromagnetic S Magnetometer 10 Days Electromagnetic S Magnetometer 81

S 40 Days Geology ' 20 Days Geology KRL 939110 KRL 939113

No credits have been allowed for the following mining claims

| | not sufficiently covered by the survey [ | insufficient technical data filed


828 (B5HZ)

Ministry ofNorthern Development

Mines


Date

September 21, 198;

File

2.10185Mining Recorder's Report of Work No.

66-87

Recorded Holder

Noranda Exploration Company Limited

Slate LakeType of survey and number of

Assessment days credit per claimGeophysical

Flertrnmagnetir ^-" days

20Magnetometer days


Geological 41) days

Gfiorheminal 4 days

Man days |~3 Airborne |~]

Special provision Q Ground fXj

j | Credits have been reduced because of partial coverage of claims.



KRL 926983 - 985 927017 939107 939111

Special credits under section 77 (16) for the following mining claims

10 Days Electromagnetics Magnetometer and 20 Days Geology and 4 Days Geochemical KRL 926986

15 Days Electromagnetic b Magnetometer and 40 days Geology and 4 Days Geochemical KRL 939099 - 100; KRL 939104 - 105

10 Days Electromagnetic S Magnetometer and 40 Days Geology and 4 Days Geochemical KRL 939106; KRL" 939108 - 109

No credits have been allowed for the following mining claims

| ) not sufficiently covered by the survey | | insufficient technical data filed


eze

October 7, 1987 Your File: 64,65,66-87 Our File: 2.10185

Mining RecorderMinistry of Northern Development and MinesP.O. Box 324Red Lake, OntarioPOV 2MO

Dear Sir:

RE: Notice of Intent dated September 21, 1987Geophysical (Electromagnetic and Magnetometer), Geological and Geochemical Surveys on Mining Claims KRL 926983, et al. 1n Slate Lake Area-————————.

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so Indicate on your records.

Yours sincerely,

R.M. Charnesky (Mrs.)Acting ManagerMining Lands SectionMineral Development and Lands BranchMines and Minerals Division

Whitney Block, Room 6610 Queen's Park Toronto, Ontario M7A 1W3

Telephone: (416) 965-4888

RM:pl

cc: Noranda Exploration CompaP.O. Bos 2656 t Thunder Bay, Ontario P7B 5G2

Mr. G.K. FergusonMining and Lands Comm1ss1oToronto, Ontario

UCHI L AKE and

EARNGEY TWP.

KRL. l KRL j KRL

BOWERMAN : : TWPFOR .STATUS REFER TO -r ~, TWP PLAN

^ T^.TT t\ e r~L -t l J U L" ir -f y .-F.Q7 l T 7,^f ' n '

WHITEMUD LAKE G

T—5! 000

ro

O

UJ

500 52 30

920 30

REFERENCES

AREAS WITHDRAWN"-FROM D ISPOSITION

'j M.R.O.-MINING RIGHTSONLY ^

S.R.O. - SLTRFACE RIGHTS ONLY - * .- ?

.M.+ S, - MINING AND SURFACE RIGHTS-•c.'.

Description Order No. D*ta Diiposition

LEGENDHIGHWAY AND ROUTE No.

OTHER ROADS '

TRAIL'S

SURVEYED LINES:TOWNSHIPS, BASE LINIS. ETC.LOTS, MINING CLAIMS. PARCELS. ETC

UNSURVEYED LINES:LOT LINESPARCEL BOUNDARYMINING C LAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY L INES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION O R COMPOSITE P LAN

RESERVATIONS

^ORIGINAL S HORELINE

MARSH OR MUSKEG

MINES

TRAVERSE MONUMENT

'///////////////////////A

DfSPOSmON OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT, SURFACE & MINING RIGHTS.._...,.^^..m 0

.SURFACE RIGHTS ONLY_.......__.^__. ©

, MINING RIGHTS ONLY __............™..._. O

LEASE, SURFACE S MINING RIGHTS...—..-,——l-__. O

" .SURFACE RIGHTS ONLY—....,.....,,-™...__. H

" .MINING RIGHTSONLY......._L.__,.-..__. B

LICENCE OF OCCUPATION ,._....____.___,-__. T-

ORDER-fN-COUNCIL ™......................._——— OC

RESERVATION .^__....^...,............__^-..___. ©

CANCELLED ___^.....,.......................—__ ®

SAND St G RAVEL .__,m.__...J....._._,....™^.. Q

NOTE: MIMING RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6. 1913. VESTED IN ORIGINAL PATENTEE Br THE ^UBLlC. LANDS ACT. B.S.O. 1970, CHAP MO. SEC 63, SU8SEC 1-

SCAlt: 1 flMCH ^ 40 CHAINS

O 10OO 7OOO eooo aooo

o ?ooMETRES

1OOO1 KM:

20OO|2 KM)

AREA

E I L

M.N.R. ADMINISTRATIVE DISTRICT

RED LAKEMIKING D IVISION

RED LAKELAKD TITLES/ REGISTRY D IVISION

KENORA/PATRiCIA

Ministry of Natural

Land -Ma n ag em en t

OntarioResources - B ranch J /'

~-*r r- J IKMX

Ditt FEB. 1963

4

50 s L

LOCATION MAP

l - 1,600,000

52 K

tt*

52K15NE0016 2.10185 SLATE LAKE ai0

REVISED

PROJ.No.NTS/ 5? K

SCALE

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HUMUS SAMPLING MAP

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PROJECT' PANAMA LAKE

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norandaNORANDA EXPLORATION Co LTD. - THUNDER BAY

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100m (Om to 100m 200m1 f 1 ' f ^ 1

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F^MJl^ LAJiS1MAGNETOMETER SURVEY

i

PROJECT: PANAMA LAKE PROJECT # : 1322.BASELINE AZIMUTH : 55 Deg.

SCALE ^ 1: 5000 DATE : 10/26/86SURVEY BY : JM NTS : 52 K/ 15

FILE: W1322PALNORANDA EXPLORATION i

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Contour Interval : " 00 nT

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( 1 passes through o .'J pt. Manning Filter.

Conductor Axis :

IWm Urn Omi i i i i

100ml

800m

S2K15NEOei6 2.10185 SLATE LAKE 230

PANAMA LAKEMAGNETOMETER SURVEY

( FILTERED CONTOUR PRESENTATION )

PROJECT: PANAMA L^KE PROJECT # : 1322, BASELINE AZIMUTH : 55 Deg.

SCALE ^ 1: 5000 DATE : 10/26/86

SURVEY BY : JM NTS : 52 K/15

FILE: M1322PAL NORANDA EXPLORATION

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Tx Location : NLK Seattle, Wash. Contour Interval :

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100mi

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PANAMAVLF SURVEY

PROJECT : PANAMA UVKE BASELINE AZIMUTH

PROJECT # 55 Deg.

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NORANDA EXPLORATION

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UJo o oo

o o oCM

UJooCM CM'

IjJ Oo

900N.

700N..

500N..

DOS

300S..

BASELINE

700:

Tx Location : NLK Seattle, W ash.

Contour Interval : 10.0 X

( 1 posbea through a 9 pt. Manning Filter.)

( ' passes through a 3 pt. Manning Filter.)

Fraser Filter on In —Phase Component

100m 60m Omi i i i i

100mi

200m-J

52KI5NE0016 2.18185 SLATE LAKE E50

VLF SURVEY( FILTERED CONTOUR PRESENTATION )

PROJECT : PANAMA LAKE PROJECT # : 1322 BASELINE AZIMUTH : 55 Deg.

SCALE = 1 : 5000 SURVEY BY : RS FILE: V1322PAN

DATE : 132/ O/ ONTS : 52 D/6FREQ.: 21.8 KHz.

NORANDA EXPLORATION

J.I1 fc* 1 f* 1 M7 at lfl*37 UMn rf ptot (rt 1 000, Of X 1I7.AN ftvM ^ VH140. UMT t HOHWCM

^

PANAMA L AKE

LOCATION MAP

: 1,600,000

52 K

t?

GABBRO

MAFIC TUFF

OXIDE IRON FORMATION

BANDED ARGILLITE- GREYWACKE (TUFFACEOUS)

INTERMEDIATE TO FELSIC TUFF

MAFIC VOLCANIC (FLOW

*

- OUTCROP

: GEOLOGICAL CONTACT

- CLAIM POST (LOCATED)

: CLAIM POST (ASSUMED)

- CLAIM LINE

- CREEK-FLOW DIRECTION INDICATED

: SWAMP

: SILICIFIED SHEAR ZONE

GEOLOGY

PROJECT PANAMA L AKEDRAWN BY R. K. DATE: J AN 1987

52K15NE00I6 2 .10185 SLATE LAKEnoranda

NORANDA EXPLORATION Co. LTD. - THUNDER BAY

noranda exploration company, limited · 2017-01-17 · noranda exploration company, limited (no...

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